Concept information
اصطلاح مرجح
وارونگی زمینی
نوع
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http://www.irandoc.ac.ir/onto/irandoc-meta/Concept
مفهوم اعم
تعاریف
- An air layer with its base at the ground surface and in which temperature increases with height. These often form at night over land under clear skies and are statically stable. See inversion, lapse rate.
منسوخ
- false
در زبان های دیگر
-
English
URI
http://www.irandoc.acir/onto/irandoc/SWEETT03756
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